6.3.2 Gravity: A Force

The idea of gravity has a long and interesting history intertwined with our evolving ideas about the solar system. It was Newton who—along with discovering his three laws of motion—first recognized that gravity is an attractive, long-range force between any two objects.

FIGURE 6.6 shows two objects with masses m1 and m2 separated by distance r. Each object pulls on the other with a force given by Newton’s law of gravity:

F1 on 2=F2 on 1=Gm1m2r2  (Newton’s law of gravity) (6.3)

where G=6.67×10−11 N m2/kg2, called the gravitational constant, is one of the basic constants of nature. Notice that gravity is not a constant force—the force gets weaker as the distance between the objects increases.

FIGURE 6.6 Newton’s law of gravity.

The figure illustrates the characteristics of the force vectors acting on two masses labeled m subscript 1 and m subscript 2.
FIGURE 6.6 Full Alternative Text

The gravitational force between two human-sized objects is minuscule, completely insignificant in comparison with other forces. That’s why you’re not aware of being tugged toward everything around you. Only when one or both objects are planet-sized or larger does gravity become an important force. Indeed, Chapter 13 will explore in detail the application of Newton’s law of gravity to the orbits of satellites and planets.

For objects moving near the surface of the earth (or other planet), things like balls and cars and planes that we’ll be studying in the next few chapters, we can make the flat-earth approximation shown in FIGURE 6.7. That is, if the object’s height above the surface is very small in comparison with the size of the planet, then the curvature of the surface is not noticeable and there’s virtually no difference between r and the planet’s radius R. Consequently, a very good approximation for the gravitational force of the planet on mass m is simply

F⃗G=F⃗planet on  m=(GMmR2, straight down)=(mg, straight down) (6.4)

FIGURE 6.7 Gravity near the surface of a planet.

The figure illustrates the flat earth approximation for an object near the surface of a planet.
FIGURE 6.7 Full Alternative Text

The magnitude or size of the gravitational force is FG=mg, where the quantity g—a property of the planet—is defined to be

g=GMR2 (6.5)

Also, the direction of the gravitational force defines what we mean by “straight down.”

But why did we choose to call it g, a symbol we’ve already used for free-fall acceleration? To see the connection, recall that free fall is motion under the influence of gravity only. FIGURE 6.8 shows the free-body diagram of an object in free fall near the surface of a planet. With F⃗net=F⃗G, Newton’s second law predicts the acceleration to be

a⃗free fall=F⃗netm=F⃗Gm=(g, straight down) (6.6)

Because g is a property of the planet, independent of the object, all objects on the same planet, regardless of mass, have the same free-fall acceleration. We introduced this idea in Chapter 2 as an experimental discovery of Galileo, but now we see that the mass independence of a⃗free fall is a prediction of Newton’s law of gravity.

FIGURE 6.8 The free-body diagram of an object in free fall.

The figure illustrates the free-body diagram of an object in free fall on the x y coordinate plane.
FIGURE 6.8 Full Alternative Text

But does Newton’s law predict the correct value, which we know from experiment to be g=|afree fall|=9.80 m/s2? We can use the average radius (Rearth=6.37×106 m) and mass (Mearth=5.97×1024 kg) of the earth to calculate

gearth=GMearth(Rearth)2=(6.67×10−11 N m2/kg2)(5.97×1024 kg)(6.37×106 m)2=9.82 N/kg

You should convince yourself that N/kg is equivalent to m/s2, so gearth=9.82 m/s2.

NOTE   Astronomical data are provided in the Useful Data.

Newton’s prediction is very close, but it’s not quite right. The free-fall acceleration would be 9.82 m/s2 on a stationary earth, but, in reality, the earth is rotating on its axis. The “missing” 0.02 m/s2 is due to the earth’s rotation, a claim we’ll justify when we study circular motion in Chapter 8. Because we’re on the outside of a rotating sphere, rather like being on the outside edge of a merry-go-round, the effect of rotation is to “weaken” gravity.

Strictly speaking, Newton’s laws of motion are not valid in an earth-based reference frame because it is rotating and thus is not an inertial reference frame. Fortunately, we can use Newton’s laws to analyze motion near the earth’s surface, and we can use FG=mg for the gravitational force if we use g=|afree fall|=9.80 m/s2 rather than g=gearth. (This assertion is proved in more advanced classes.) In our rotating reference frame, F⃗G is the effective gravitational force, the true gravitational force given by Newton’s law of gravity plus a small correction due to our rotation. This is the force to show on free-body diagrams and use in calculations.